Journal article 1674 views
Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint
Inger K. Seierstad,
Peter Abbott
,
Matthias Bigler,
Thomas Blunier,
Anna Bourne
,
Edward Brook,
Susanne L. Buchardt,
Christo Buizert,
Henrik B. Clausen,
Eliza Cook,
Dorthe Dahl-Jensen,
Siwan Davies
,
Myriam Guillevic,
Sigfús J. Johnsen,
Desirée S. Pedersen,
Trevor J. Popp,
Sune O. Rasmussen,
Jeffrey P. Severinghaus,
Anders Svensson,
Bo M. Vinther
Quaternary Science Reviews, Volume: 106, Pages: 29 - 46
Swansea University Authors:
Peter Abbott , Anna Bourne
, Siwan Davies
Full text not available from this repository: check for access using links below.
DOI (Published version): 10.1016/j.quascirev.2014.10.032
Abstract
Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint
| Published in: | Quaternary Science Reviews |
|---|---|
| ISSN: | 0277-3791 |
| Published: |
Elsevier BV
2014
|
| Online Access: |
Check full text
|
| URI: | https://cronfa.swan.ac.uk/Record/cronfa19598 |
| Keywords: |
Paleoclimate; Greenland ice cores; GICC05 chronology; Tephra isochrons; Regional climate; Water isotopes (δ18O); Heinrich event |
|---|---|
| College: |
Faculty of Science and Engineering |
| Start Page: |
29 |
| End Page: |
46 |

